(Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ...
This paper presents the morpho-sedimentary characterization and interpretations of the assemblage of landforms of the East Greenland continental slope and Greenland Basin, based on swath bathymetry and sub-bottom TOPAS profiles. The interpretation of landforms reveals the glacial influence on recent...
Main Authors: | , , , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2012
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.810150 https://doi.pangaea.de/10.1594/PANGAEA.810150 |
id |
ftdatacite:10.1594/pangaea.810150 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.810150 2024-09-15T18:04:20+00:00 (Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... García, Marga M Dowdeswell, Julian A Ercilla, Gemma Jakobsson, Martin 2012 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.810150 https://doi.pangaea.de/10.1594/PANGAEA.810150 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2012.06.016 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Site Sector Gradient Height above sea floor/altitude Lake, length Froude number, internal Layer thickness Flow speed Calculated JR20000727 James Clark Ross International Polar Year 2007-2008 IPY dataset Supplementary Dataset Dataset 2012 ftdatacite https://doi.org/10.1594/pangaea.81015010.1016/j.quascirev.2012.06.016 2024-08-01T10:51:52Z This paper presents the morpho-sedimentary characterization and interpretations of the assemblage of landforms of the East Greenland continental slope and Greenland Basin, based on swath bathymetry and sub-bottom TOPAS profiles. The interpretation of landforms reveals the glacial influence on recent sedimentary processes shaping the seafloor, including mass-wasting and turbidite flows. The timing of landform development points to a predominantly glacial origin of the sediment supplied to the continental margin, supporting the scenario of a Greenland Ice Sheet extending across the continental shelf, or even to the shelf-edge, during the Last Glacial Maximum (LGM). Major sedimentary processes along the central section of the eastern Greenland Continental Slope, the Norske margin, suggest a relatively high glacial sediment input during the LGM that, probably triggered by tectonic activity, led to the development of scarps and channels on the slope and debris flows on the continental rise. The more southerly ... : Positions approximate. For a more detailed view on the transects see Figure 10 of the article. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Dataset East Greenland Greenland Ice Sheet International Polar Year IPY DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Site Sector Gradient Height above sea floor/altitude Lake, length Froude number, internal Layer thickness Flow speed Calculated JR20000727 James Clark Ross International Polar Year 2007-2008 IPY |
spellingShingle |
Site Sector Gradient Height above sea floor/altitude Lake, length Froude number, internal Layer thickness Flow speed Calculated JR20000727 James Clark Ross International Polar Year 2007-2008 IPY García, Marga M Dowdeswell, Julian A Ercilla, Gemma Jakobsson, Martin (Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
topic_facet |
Site Sector Gradient Height above sea floor/altitude Lake, length Froude number, internal Layer thickness Flow speed Calculated JR20000727 James Clark Ross International Polar Year 2007-2008 IPY |
description |
This paper presents the morpho-sedimentary characterization and interpretations of the assemblage of landforms of the East Greenland continental slope and Greenland Basin, based on swath bathymetry and sub-bottom TOPAS profiles. The interpretation of landforms reveals the glacial influence on recent sedimentary processes shaping the seafloor, including mass-wasting and turbidite flows. The timing of landform development points to a predominantly glacial origin of the sediment supplied to the continental margin, supporting the scenario of a Greenland Ice Sheet extending across the continental shelf, or even to the shelf-edge, during the Last Glacial Maximum (LGM). Major sedimentary processes along the central section of the eastern Greenland Continental Slope, the Norske margin, suggest a relatively high glacial sediment input during the LGM that, probably triggered by tectonic activity, led to the development of scarps and channels on the slope and debris flows on the continental rise. The more southerly ... : Positions approximate. For a more detailed view on the transects see Figure 10 of the article. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... |
format |
Dataset |
author |
García, Marga M Dowdeswell, Julian A Ercilla, Gemma Jakobsson, Martin |
author_facet |
García, Marga M Dowdeswell, Julian A Ercilla, Gemma Jakobsson, Martin |
author_sort |
García, Marga M |
title |
(Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
title_short |
(Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
title_full |
(Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
title_fullStr |
(Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
title_full_unstemmed |
(Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
title_sort |
(table 2) characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves ... |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.810150 https://doi.pangaea.de/10.1594/PANGAEA.810150 |
genre |
East Greenland Greenland Ice Sheet International Polar Year IPY |
genre_facet |
East Greenland Greenland Ice Sheet International Polar Year IPY |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2012.06.016 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.81015010.1016/j.quascirev.2012.06.016 |
_version_ |
1810441821210279936 |